Wrenching Tectonism in the Southernmost Andes and the Scotia Sea Constrained from Fault Kinematic and Seismotectonic Overviews

The geodynamics of the study area includes subduction, orogen dynamics, and major transcurrent tectonics at a complex transform margin in the southern ocean. We present a synthesis of the fault system associated to major fault zones in the Fuegian Andes and the Scotia Sea and review the available ki...

Full description

Bibliographic Details
Main Authors: Sue, Christian, Ghiglione, Matias
Format: Book Part
Language:English
Published: Springer
Subjects:
Online Access:http://hdl.handle.net/11336/105119
_version_ 1821563357745905664
author Sue, Christian
Ghiglione, Matias
author2 Ghiglione, Matias
author_facet Sue, Christian
Ghiglione, Matias
author_sort Sue, Christian
collection CONICET Digital (Consejo Nacional de Investigaciones Científicas y Técnicas)
container_start_page 137
description The geodynamics of the study area includes subduction, orogen dynamics, and major transcurrent tectonics at a complex transform margin in the southern ocean. We present a synthesis of the fault system associated to major fault zones in the Fuegian Andes and the Scotia Sea and review the available kinematic databases from microtectonic measurements. Our synthesis of six independent fault kinematic studies is coherent with a very consistent shortening direction-oriented NE–SW in the Southernmost Andes. The stability of the stress pattern and orientation of the shortening axes on a more regional scale involving the Scotia Sea indicate a steady E–W to NNE–SSW σ1/shortening direction since middle Eocene times. This observations reflect that the global left-lateral motion between Antarctica–Scotia–South America plates circuit is the main driving force for the entire area and in particular for the Southernmost Andes, over the last ~45 Ma. Both the observed short-term geodetic and the long-term geological slip rates of the Magallanes–Fagnano fault system from Tierra del Fuego are moderate (~5 mm/year), and the expected time span between major M8 earthquakes would be around 10 kyr. Yet the time between the two most recent large earthquakes was about 70 years. Such a great discrepancy suggests a complex mechanics on the Magallanes–Fagnano fault system, leading to complex recurrence time history for the characteristic earthquake (M ≥ 7). Fil: Sue, Christian. Universite de Bourgogne; Francia Fil: Ghiglione, Matias. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Estudios Andinos "Don Pablo Groeber". Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Estudios Andinos "Don Pablo Groeber"; Argentina
format Book Part
genre Antarc*
Antarctica
Scotia Sea
Southern Ocean
Tierra del Fuego
genre_facet Antarc*
Antarctica
Scotia Sea
Southern Ocean
Tierra del Fuego
geographic Southern Ocean
Scotia Sea
Argentina
Magallanes
Pablo
geographic_facet Southern Ocean
Scotia Sea
Argentina
Magallanes
Pablo
id ftconicet:oai:ri.conicet.gov.ar:11336/105119
institution Open Polar
language English
long_lat ENVELOPE(-62.933,-62.933,-64.883,-64.883)
ENVELOPE(-63.717,-63.717,-64.283,-64.283)
op_collection_id ftconicet
op_container_end_page 171
op_doi https://doi.org/10.1007/978-3-319-39727-6_6
op_relation info:eu-repo/semantics/altIdentifier/url/https://link.springer.com/chapter/10.1007/978-3-319-39727-6_6
info:eu-repo/semantics/altIdentifier/doi/10.1007/978-3-319-39727-6_6
http://hdl.handle.net/11336/105119
Sue, Christian; Ghiglione, Matias; Wrenching Tectonism in the Southernmost Andes and the Scotia Sea Constrained from Fault Kinematic and Seismotectonic Overviews; Springer; 2016; 137-171
978-3-319-39725-2
CONICET Digital
CONICET
op_rights info:eu-repo/semantics/restrictedAccess
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
publisher Springer
record_format openpolar
spelling ftconicet:oai:ri.conicet.gov.ar:11336/105119 2025-01-16T19:05:35+00:00 Wrenching Tectonism in the Southernmost Andes and the Scotia Sea Constrained from Fault Kinematic and Seismotectonic Overviews Sue, Christian Ghiglione, Matias Ghiglione, Matias application/pdf http://hdl.handle.net/11336/105119 eng eng Springer info:eu-repo/semantics/altIdentifier/url/https://link.springer.com/chapter/10.1007/978-3-319-39727-6_6 info:eu-repo/semantics/altIdentifier/doi/10.1007/978-3-319-39727-6_6 http://hdl.handle.net/11336/105119 Sue, Christian; Ghiglione, Matias; Wrenching Tectonism in the Southernmost Andes and the Scotia Sea Constrained from Fault Kinematic and Seismotectonic Overviews; Springer; 2016; 137-171 978-3-319-39725-2 CONICET Digital CONICET info:eu-repo/semantics/restrictedAccess https://creativecommons.org/licenses/by-nc-sa/2.5/ar/ GPS FAULT KINEMATICS MAGALLANES FAGNANO FAULT SCOTIA ARC https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 info:eu-repo/semantics/publishedVersion info:eu-repo/semantics/bookPart info:ar-repo/semantics/parte de libro ftconicet https://doi.org/10.1007/978-3-319-39727-6_6 2023-09-24T19:50:07Z The geodynamics of the study area includes subduction, orogen dynamics, and major transcurrent tectonics at a complex transform margin in the southern ocean. We present a synthesis of the fault system associated to major fault zones in the Fuegian Andes and the Scotia Sea and review the available kinematic databases from microtectonic measurements. Our synthesis of six independent fault kinematic studies is coherent with a very consistent shortening direction-oriented NE–SW in the Southernmost Andes. The stability of the stress pattern and orientation of the shortening axes on a more regional scale involving the Scotia Sea indicate a steady E–W to NNE–SSW σ1/shortening direction since middle Eocene times. This observations reflect that the global left-lateral motion between Antarctica–Scotia–South America plates circuit is the main driving force for the entire area and in particular for the Southernmost Andes, over the last ~45 Ma. Both the observed short-term geodetic and the long-term geological slip rates of the Magallanes–Fagnano fault system from Tierra del Fuego are moderate (~5 mm/year), and the expected time span between major M8 earthquakes would be around 10 kyr. Yet the time between the two most recent large earthquakes was about 70 years. Such a great discrepancy suggests a complex mechanics on the Magallanes–Fagnano fault system, leading to complex recurrence time history for the characteristic earthquake (M ≥ 7). Fil: Sue, Christian. Universite de Bourgogne; Francia Fil: Ghiglione, Matias. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Estudios Andinos "Don Pablo Groeber". Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Estudios Andinos "Don Pablo Groeber"; Argentina Book Part Antarc* Antarctica Scotia Sea Southern Ocean Tierra del Fuego CONICET Digital (Consejo Nacional de Investigaciones Científicas y Técnicas) Southern Ocean Scotia Sea Argentina Magallanes ENVELOPE(-62.933,-62.933,-64.883,-64.883) Pablo ENVELOPE(-63.717,-63.717,-64.283,-64.283) 137 171
spellingShingle GPS
FAULT KINEMATICS
MAGALLANES FAGNANO FAULT
SCOTIA ARC
https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
Sue, Christian
Ghiglione, Matias
Wrenching Tectonism in the Southernmost Andes and the Scotia Sea Constrained from Fault Kinematic and Seismotectonic Overviews
title Wrenching Tectonism in the Southernmost Andes and the Scotia Sea Constrained from Fault Kinematic and Seismotectonic Overviews
title_full Wrenching Tectonism in the Southernmost Andes and the Scotia Sea Constrained from Fault Kinematic and Seismotectonic Overviews
title_fullStr Wrenching Tectonism in the Southernmost Andes and the Scotia Sea Constrained from Fault Kinematic and Seismotectonic Overviews
title_full_unstemmed Wrenching Tectonism in the Southernmost Andes and the Scotia Sea Constrained from Fault Kinematic and Seismotectonic Overviews
title_short Wrenching Tectonism in the Southernmost Andes and the Scotia Sea Constrained from Fault Kinematic and Seismotectonic Overviews
title_sort wrenching tectonism in the southernmost andes and the scotia sea constrained from fault kinematic and seismotectonic overviews
topic GPS
FAULT KINEMATICS
MAGALLANES FAGNANO FAULT
SCOTIA ARC
https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
topic_facet GPS
FAULT KINEMATICS
MAGALLANES FAGNANO FAULT
SCOTIA ARC
https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
url http://hdl.handle.net/11336/105119